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Graded Streams: Considering the longitudinal (downstream) profile of a stream: Where a stream flows down a steep slope velocity will increase which will result in increased erosion. Where that stream then Velocity River Increase Downstream flows onto a gentler slope velocity decreases and deposition will result. Apr 20, �� The velocity of a river is determined by many factors, including the shape of its channel, the gradient of the slope that the river moves along, the volume of water that the river carries and the amount of friction caused by rough edges within the riverbed. The velocity can change at various points along the course of a river. How does a river change course downstream? A river changes shape as it flows from its source to its mouth. A section of the course of a river drawn from source to mouth is known as a long profile.

In straight channels, highest velocity is in the center. During a flood discharge exceeds the storage volume of the stream channel. For example, deforestation changed urbanization lead to the excavation of sand and stones for building along riverbeds. Red Panda Facts. Drainage reversals can occur as a result of tectonic processes.




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